The model for
source-receptor distances of the order of kilometers
was evaluated with data derived from two tracer experiments
conducted during August and December of 2001 at Barrio
Logan, San Diego. |
Observed turbulent intensities vary by
less
than 20% in the vertical in the boundary layer |
|
Model performance when initial
spreads
are taken to be zero
|
|
|
|
|
|
Better model performance
when initial
horizontal spread is taken to be 50m
It's necessary
to account for initial plume
spread caused by building effects to explain concentrations on the 200m
and 500m arcs. |
Model performance based on turbulent intensities
averaged over the entire field study is almost as well as
the
model performance using experiment specific meteorology
|
|
Venkatram, A., Isakov,
V., Pankratz, D., and
Yuan, J., 2005: Relating plume spread to meteorology in urban areas. Atmospheric Environment, 39(2), 371-380
Venkatram, A., Isakov, V., Yuan, J., Pankratz, D., 2004: Modeling
dispersion at distances of meters from urban sources. Atmospheric
Environment, 38, 4633-4641
Venkatram, A.,
Isakov, V., Pankratz, D., Heumann, J., and Yuan, J., 2004: The analysis of data
from an urban dispersion experiment. Atmospheric Environment, 38(22),
3647-3659
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